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Air Quality this morninghttp://utahaq.chpc.utah.edu/

PM2.5 Ozone

Meteorology-Chemistry Coupling in Western

Basins What’s similar, what’s

different, what’s missing? John Horel1, Erik Crosman2, Sebastian Hoch1

1University of Utah2West Texas A&M

with contributions from: Alex Jacques & Brian Blaylock, others in the

Mountain Meteorology Group

Meteorology-Chemistry Coupling in Western

Basins What’s similar, what’s

different, what’s missing? John Horel1, Erik Crosman2, Sebastian Hoch1

1University of Utah2West Texas A&M

with contributions from: Alex Jacques & Brian Blaylock, others in the

Mountain Meteorology Group

700 hPa Wind

Meteorology-Chemistry Coupling in Western

Basins What’s similar, what’s

different, what’s missing?

Blue: Valley & Basin Cold-Air Pools

John Horel1, Erik Crosman2, Sebastian Hoch1

1University of Utah2West Texas A&M

with contributions from: Alex Jacques & Brian Blaylock among others in

the Mountain Meteorology Group

2 m Potential Temperature

Geometry, land-use & populationEmission sources

Surface state: snow-covered or wet/dryExisting resources & flight restrictions

Synoptic/mesoscale controlsFree atmos.-boundary layer exchanges Lateral transport within boundary layer

Terrain-flow interactionsStructure/turbulence in boundary layer

Water/ice clouds & depositionMeteorology

Air Chemistry

Basins & Valleys

V 10mi

Oakland

Temperature (◦C)

Pres

sure

Temperature (◦C)

Vertical StructureJanuary 31,2017 12 UTC

Blue: Valley & Basin Cold-Air Pools

V 10 mi

V 10mi

Oakland

Temperature (◦C)

RenoPr

essu

rePr

essu

re

Temperature (◦C)

Vertical StructureJanuary 31,2017 12 UTC

Blue: Valley & Basin Cold-Air Pools

V 10 mi

V 10miHazeV 5mi

Boise

Pres

sure

Oakland

Temperature (◦C)

Temperature (◦C)

RenoPr

essu

rePr

essu

re

Temperature (◦C)

Vertical StructureJanuary 31,2017 12 UTC

Blue: Valley & Basin Cold-Air Pools

V 10 mi

V 10mi

FogV 3 mi

HazeV 5mi

Boise

Salt Lake City

Pres

sure

Pres

sure

Oakland

Temperature (◦C)

Temperature (◦C)Temperature (◦C)

RenoPr

essu

rePr

essu

re

Temperature (◦C)

Vertical StructureJanuary 31,2017 12 UTC

Blue: Valley & Basin Cold-Air Pools

January 31, 2017San Joaquin Valley

Temperature (oC)

January 31, 2017Salt Lake Valley

Temperature (oC)

PM2.5

Boundary layer & slope flow evolution in the Salt Lake Valley: Jan. 31, 2017Hoch & Crosman

NSF RAPID / METEOROLOGY DURING UWFPS~12 UTC

“FoggyCloudy”

“Clear”“Clear”

Night-time injection of low-PM2.5, high O3 air is reduced

January 31, 2017Cache Valley, UT

Temperature (oC)

• Large-scale flow aloft• Conditions evolving

diurnally & over lifetime of pollution event

Similarities

• Snow cover• Temperature regime• Boundary layer depth• Fog/stratus• Terrain, slope and

intrabasin flows

Differences

• Temperature dependent reactions

• Heterogeneous, aqueous (warm/ice) phase chemistry

• Changes in night-time injection of low-PM2.5 & high O3

Impacts

January 31, 2017

Planning & Situational Awareness Resources: PM2.5

> 700 state/county locations 16 DAQ/UUtah> 90 AirU sites; ~400 Purple Air

> 130 CARB/county> ~1400 Purple Air

Planning & Situational Awareness Resources: Surface Wind Observations

> 7500 locations > 300 locations> 1300 locations

Planning & Situational Awareness• Synoptic/mesoscale conditions

usually simulated adequately by operational models

• But…• Breakup phase harder to forecast

than onset• Transition from clear-air to cloudy

boundary layers (and vice versa) difficult

• Boundary layer processes tend to be overly dispersive/damped

2 m Relative Humidity

Planning & Situational Awareness• Considerable work underway using

research model simulations• Improved treatment of boundary

layer processes needed for:• Convection-Allowing Models (1-3 km) • Large-Eddy Simulations (10’s-100’s m)

Wilson and Fovell 2018, WAF

Summary• Boundary layer meteorology/air chemistry processes are too

intertwined to treat independently• Understanding pollutant events from beginning to end requires close

collaboration to understand how chemical species evolve as the conditions evolve

• Complexity of events in all basins requires:• taking advantage of existing sensor networks• deploying diverse sensor types and using innovative deployment strategies to

fill in the gaps (e.g., plane, in situ and surface-based remote, mobile, drones, IOTs)

• having the science plan factor in the strengths & weaknesses of sensor types to evolving boundary layer conditions

Links to Resources

• Web resources • MesoWest: https://mesowest.utah.edu• Utah air quality: http://utahaq.chpc.utah.edu/• LAIR group: https://air.utah.edu/

• Data Archives • Surface observational data: https://synopticdata.com/• HRRR analyses: http://hrrr.chpc.utah.edu/

Recent Related Publications• Mitchell, L. E., and Coauthors, 2018: Monitoring of Greenhouse Gases and Pollutants across an

Urban Area using a Light-rail Public Transit Platform. Atmos. Env., 187, 9-23, doi:10.1016/j.atmosenv.2018.05.044

• Lin, J. C., and Coauthors, 2018: CO2 and Carbon Emissions from Cities: Linkages to Air Quality, Socioeconomic Activity and Stakeholders in the Salt Lake City Urban Area. Bull. Amer. Meteor. Soc., 99, 2325-2339, doi:10.1175/BAMS-D-17-0037.1

• Franchin, A., and Coauthors, 2018: Airborne and ground based observations of aerosol chemical and physical properties during intense winter pollution episodes in the Great Salt Lake Basin, Atmospheric Chemistry and Physics, 18, 17259-17276. https://www.atmos-chem-phys.net/18/17259/2018/

• Foster, C., and Coauthors, 2018: Constraining methane emissions in Utah’s Uintah Basin with ground-based observations and a time-reversed Lagrangian transport model. J. Geophys. Res. Atmos. 122, https://doi.org/10.1002/2017JD027480.

• Crosman, E., A. Jacques, J. Horel, 2017: A Novel Approach for Monitoring Vertical Profiles of Boundary-Layer Pollutants: Utilizing Routine News Helicopter Flights. Atmospheric Pollution Research. 8, 828-835. http://dx.doi.org/10.1016/j.apr.2017.01.013

• Foster, C., E. Crosman, J. Horel, 2017: Simulations of a Cold-Air Pool in Utah’s Salt Lake Valley: Sensitivity to Land Use and Snow Cover. Boundary Layer Meteorology. 164, 63-87. http://dx.doi.org/10.1007/s10546-017-0240-7

• Crosman, E., J. Horel, 2017: Large-eddy simulations of a Salt Lake Valley cold-air pool. Atmospheric Research. 193, 10–25. http://10.1016/j.atmosres.2017.04.010